Not listed DEVELOPMENT OF BAROTROPIC AND BAROCLINIC TIDE MODELS IN SUPPORT OF THE SWOT MISSION THE SURFACE WATER AND OCEAN TOPOGRAPHY (SWOT) MISSION WILL OPEN A NEW WINDOW TO THE REMOTE SENSING OF WATER OVER BOTH INLAND WATER BODIES AND THE GLOBAL OCEAN (DURAND ET AL. 2010). FOR THE OCEAN THAT NEW WINDOW WILL BE HIGH-WAVENUMBER DYNAMIC TOPOGRAPHY HERETOFORE NEVER DIRECTLY MEASURED. THESE NEW SUBMESOSCALE MEASUREMENTS OF SEA-SURFACE HEIGHTS SHOULD ALLOW FOR THE FIRST TIME A QUANTITATIVE STUDY OF THE OCEAN AT SCALES THOUGHT CRITICAL FOR UNDERSTANDING TURBULENCE AND ENERGY DISSIPATION (FU & FERRARI 2008). AS WITH ANY NEW KIND OF SATELLITE MEASUREMENT THERE ARE MANY TECHNICAL AND SCIENTIFIC HURDLES THAT MUST BE OVERCOME TO MEET MISSION GOALS. THIS PROPOSAL IS DEVOTED TO ONE OF THEM TIDES WHICH HAS THE POTENTIAL TO IMPACT OUR ABILITY TO SUCCESSFULLY RECOVER SUBMESOSCALE OCEAN TOPOGRAPHY WITH ALTIMETRY (CHAVANNE & KLEIN 2010 RAY & ZARON 2011 PONTE & KLEIN 2015). THIS PROPOSAL AIMS TO: PROVIDE THE SWOT SCIENCE TEAM WITH GUIDANCE AND ADVICE REGARDING ALL ASPECTS OF TIDES. OF SPECIAL CONCERN WILL BE THE EFFECTS OF DEEP-OCEAN INTERNAL TIDES AND HOW THEY MAY OR MAY NOT HINDER MAPPING OF SUBMESOSCALE VARIABILITY. CONDUCT RESEARCH ALONG WITH MEMBERS OF THE OCEAN SURFACE TOPOGRAPHY SCIENCE TEAM (OSTST) AS WELL AS THE WIDER GEOPHYSICAL COMMUNITY INTO THE PREDICTABILITY OF DEEP-OCEAN INTERNAL TIDES. PREPARE THE GROUNDWORK FOR HANDLING FUTURE SWOT MEASUREMENTS TO ALLOW SUCCESSFUL ESTIMATION OF TIDES. THE UNPRECEDENTED HIGH SPATIAL RESOLUTION OF SWOT DATA WILL FOR EXAMPLE REQUIRE REVISION OF STANDARD METHODS FOR TIDAL DATA ASSIMILATION. HELP WITH THE DESIGN OF ALGORITHMS FOR COMPUTING TIDAL CORRECTIONS TO SWOT DATA. FOR EXAMPLE A COMPLEX FAMILY OF NESTED MODELS IS ENVISIONED IN ORDER TO PRODUCE THE MOST ACCURATE CORRECTIONS IN SHALLOW SEAS AND NEAR-COASTAL WATERS. $35.1k 3/3/20 4 DEVELOPMENT OF BAROTROPIC AND BAROCLINIC TIDE MODELS IN SUPPORT OF THE SWOT MISSION THE SURFACE WATER AND OCEAN TOPOGRAPHY (SWOT) MISSION WILL OPEN A NEW WINDOW TO THE REMOTE SENSING OF WATER, OVER BOTH INLAND WATER BODIES AND THE GLOBAL OCEAN (DURAND ET AL., 2010). FOR THE OCEAN THAT NEW WINDOW WILL BE HIGH-WAVENUMBER DYNAMIC TOPOGRAPHY HERETOFORE NEVER DIRECTLY MEASURED. THESE NEW SUBMESOSCALE MEASUREMENTS OF SEA-SURFACE HEIGHTS SHOULD ALLOW FOR THE FIRST TIME A QUANTITATIVE STUDY OF THE OCEAN AT SCALES THOUGHT CRITICAL FOR UNDERSTANDING TURBULENCE AND ENERGY DISSIPATION (FU & FERRARI, 2008). AS WITH ANY NEW KIND OF SATELLITE MEASUREMENT THERE ARE MANY TECHNICAL AND SCIENTIFIC HURDLES THAT MUST BE OVERCOME TO MEET MISSION GOALS. THIS PROPOSAL IS DEVOTED TO ONE OF THEM TIDES WHICH HAS THE POTENTIAL TO IMPACT OUR ABILITY TO SUCCESSFULLY RECOVER SUBMESOSCALE OCEAN TOPOGRAPHY WITH ALTIMETRY (CHAVANNE & KLEIN, 2010, RAY & ZARON, 2011, PONTE & KLEIN, 2015). THIS PROPOSAL AIMS TO: PROVIDE THE SWOT SCIENCE TEAM WITH GUIDANCE AND ADVICE REGARDING ALL ASPECTS OF TIDES. OF SPECIAL CONCERN WILL BE THE EFFECTS OF DEEP-OCEAN INTERNAL TIDES AND HOW THEY MAY OR MAY NOT HINDER MAPPING OF SUBMESOSCALE VARIABILITY. CONDUCT RESEARCH, ALONG WITH MEMBERS OF THE OCEAN SURFACE TOPOGRAPHY SCIENCE TEAM (OSTST) AS WELL AS THE WIDER GEOPHYSICAL COMMUNITY, INTO THE PREDICTABILITY OF DEEP-OCEAN INTERNAL TIDES. PREPARE THE GROUNDWORK FOR HANDLING FUTURE SWOT MEASUREMENTS TO ALLOW SUCCESSFUL ESTIMATION OF TIDES. THE UNPRECEDENTED HIGH SPATIAL RESOLUTION OF SWOT DATA WILL, FOR EXAMPLE, REQUIRE REVISION OF STANDARD METHODS FOR TIDAL DATA ASSIMILATION. HELP WITH THE DESIGN OF ALGORITHMS FOR COMPUTING TIDAL CORRECTIONS TO SWOT DATA. FOR EXAMPLE, A COMPLEX FAMILY OF NESTED MODELS IS ENVISIONED IN ORDER TO PRODUCE THE MOST ACCURATE CORRECTIONS IN SHALLOW SEAS AND NEAR-COASTAL WATERS. Funding Only Action $35.1k 3/3/20 3 DEVELOPMENT OF BAROTROPIC AND BAROCLINIC TIDE MODELS IN SUPPORT OF THE SWOT MISSION THE SURFACE WATER AND OCEAN TOPOGRAPHY (SWOT) MISSION WILL OPEN A NEW WINDOW TO THE REMOTE SENSING OF WATER, OVER BOTH INLAND WATER BODIES AND THE GLOBAL OCEAN (DURAND ET AL., 2010). FOR THE OCEAN THAT NEW WINDOW WILL BE HIGH-WAVENUMBER DYNAMIC TOPOGRAPHY HERETOFORE NEVER DIRECTLY MEASURED. THESE NEW SUBMESOSCALE MEASUREMENTS OF SEA-SURFACE HEIGHTS SHOULD ALLOW FOR THE FIRST TIME A QUANTITATIVE STUDY OF THE OCEAN AT SCALES THOUGHT CRITICAL FOR UNDERSTANDING TURBULENCE AND ENERGY DISSIPATION (FU & FERRARI, 2008). AS WITH ANY NEW KIND OF SATELLITE MEASUREMENT THERE ARE MANY TECHNICAL AND SCIENTIFIC HURDLES THAT MUST BE OVERCOME TO MEET MISSION GOALS. THIS PROPOSAL IS DEVOTED TO ONE OF THEM TIDES WHICH HAS THE POTENTIAL TO IMPACT OUR ABILITY TO SUCCESSFULLY RECOVER SUBMESOSCALE OCEAN TOPOGRAPHY WITH ALTIMETRY (CHAVANNE & KLEIN, 2010, RAY & ZARON, 2011, PONTE & KLEIN, 2015). THIS PROPOSAL AIMS TO: PROVIDE THE SWOT SCIENCE TEAM WITH GUIDANCE AND ADVICE REGARDING ALL ASPECTS OF TIDES. OF SPECIAL CONCERN WILL BE THE EFFECTS OF DEEP-OCEAN INTERNAL TIDES AND HOW THEY MAY OR MAY NOT HINDER MAPPING OF SUBMESOSCALE VARIABILITY. CONDUCT RESEARCH, ALONG WITH MEMBERS OF THE OCEAN SURFACE TOPOGRAPHY SCIENCE TEAM (OSTST) AS WELL AS THE WIDER GEOPHYSICAL COMMUNITY, INTO THE PREDICTABILITY OF DEEP-OCEAN INTERNAL TIDES. PREPARE THE GROUNDWORK FOR HANDLING FUTURE SWOT MEASUREMENTS TO ALLOW SUCCESSFUL ESTIMATION OF TIDES. THE UNPRECEDENTED HIGH SPATIAL RESOLUTION OF SWOT DATA WILL, FOR EXAMPLE, REQUIRE REVISION OF STANDARD METHODS FOR TIDAL DATA ASSIMILATION. HELP WITH THE DESIGN OF ALGORITHMS FOR COMPUTING TIDAL CORRECTIONS TO SWOT DATA. FOR EXAMPLE, A COMPLEX FAMILY OF NESTED MODELS IS ENVISIONED IN ORDER TO PRODUCE THE MOST ACCURATE CORRECTIONS IN SHALLOW SEAS AND NEAR-COASTAL WATERS. Funding Only Action $66.7k 5/28/19 Not listed DEVELOPMENT OF BAROTROPIC AND BAROCLINIC TIDE MODELS IN SUPPORT OF THE SWOT MISSION THE SURFACE WATER AND OCEAN TOPOGRAPHY (SWOT) MISSION WILL OPEN A NEW WINDOW TO THE REMOTE SENSING OF WATER OVER BOTH INLAND WATER BODIES AND THE GLOBAL OCEAN (DURAND ET AL. 2010). FOR THE OCEAN THAT NEW WINDOW WILL BE HIGH-WAVENUMBER DYNAMIC TOPOGRAPHY HERETOFORE NEVER DIRECTLY MEASURED. THESE NEW SUBMESOSCALE MEASUREMENTS OF SEA-SURFACE HEIGHTS SHOULD ALLOW FOR THE FIRST TIME A QUANTITATIVE STUDY OF THE OCEAN AT SCALES THOUGHT CRITICAL FOR UNDERSTANDING TURBULENCE AND ENERGY DISSIPATION (FU & FERRARI 2008). AS WITH ANY NEW KIND OF SATELLITE MEASUREMENT THERE ARE MANY TECHNICAL AND SCIENTIFIC HURDLES THAT MUST BE OVERCOME TO MEET MISSION GOALS. THIS PROPOSAL IS DEVOTED TO ONE OF THEM TIDES WHICH HAS THE POTENTIAL TO IMPACT OUR ABILITY TO SUCCESSFULLY RECOVER SUBMESOSCALE OCEAN TOPOGRAPHY WITH ALTIMETRY (CHAVANNE & KLEIN 2010 RAY & ZARON 2011 PONTE & KLEIN 2015). THIS PROPOSAL AIMS TO: PROVIDE THE SWOT SCIENCE TEAM WITH GUIDANCE AND ADVICE REGARDING ALL ASPECTS OF TIDES. OF SPECIAL CONCERN WILL BE THE EFFECTS OF DEEP-OCEAN INTERNAL TIDES AND HOW THEY MAY OR MAY NOT HINDER MAPPING OF SUBMESOSCALE VARIABILITY. CONDUCT RESEARCH ALONG WITH MEMBERS OF THE OCEAN SURFACE TOPOGRAPHY SCIENCE TEAM (OSTST) AS WELL AS THE WIDER GEOPHYSICAL COMMUNITY INTO THE PREDICTABILITY OF DEEP-OCEAN INTERNAL TIDES. PREPARE THE GROUNDWORK FOR HANDLING FUTURE SWOT MEASUREMENTS TO ALLOW SUCCESSFUL ESTIMATION OF TIDES. THE UNPRECEDENTED HIGH SPATIAL RESOLUTION OF SWOT DATA WILL FOR EXAMPLE REQUIRE REVISION OF STANDARD METHODS FOR TIDAL DATA ASSIMILATION. HELP WITH THE DESIGN OF ALGORITHMS FOR COMPUTING TIDAL CORRECTIONS TO SWOT DATA. FOR EXAMPLE A COMPLEX FAMILY OF NESTED MODELS IS ENVISIONED IN ORDER TO PRODUCE THE MOST ACCURATE CORRECTIONS IN SHALLOW SEAS AND NEAR-COASTAL WATERS. $66.7k 5/28/19 2 DEVELOPMENT OF BAROTROPIC AND BAROCLINIC TIDE MODELS IN SUPPORT OF THE SWOT MISSION THE SURFACE WATER AND OCEAN TOPOGRAPHY (SWOT) MISSION WILL OPEN A NEW WINDOW TO THE REMOTE SENSING OF WATER, OVER BOTH INLAND WATER BODIES AND THE GLOBAL OCEAN (DURAND ET AL., 2010). FOR THE OCEAN THAT NEW WINDOW WILL BE HIGH-WAVENUMBER DYNAMIC TOPOGRAPHY HERETOFORE NEVER DIRECTLY MEASURED. THESE NEW SUBMESOSCALE MEASUREMENTS OF SEA-SURFACE HEIGHTS SHOULD ALLOW FOR THE FIRST TIME A QUANTITATIVE STUDY OF THE OCEAN AT SCALES THOUGHT CRITICAL FOR UNDERSTANDING TURBULENCE AND ENERGY DISSIPATION (FU & FERRARI, 2008). AS WITH ANY NEW KIND OF SATELLITE MEASUREMENT THERE ARE MANY TECHNICAL AND SCIENTIFIC HURDLES THAT MUST BE OVERCOME TO MEET MISSION GOALS. THIS PROPOSAL IS DEVOTED TO ONE OF THEM TIDES WHICH HAS THE POTENTIAL TO IMPACT OUR ABILITY TO SUCCESSFULLY RECOVER SUBMESOSCALE OCEAN TOPOGRAPHY WITH ALTIMETRY (CHAVANNE & KLEIN, 2010, RAY & ZARON, 2011, PONTE & KLEIN, 2015). THIS PROPOSAL AIMS TO: PROVIDE THE SWOT SCIENCE TEAM WITH GUIDANCE AND ADVICE REGARDING ALL ASPECTS OF TIDES. OF SPECIAL CONCERN WILL BE THE EFFECTS OF DEEP-OCEAN INTERNAL TIDES AND HOW THEY MAY OR MAY NOT HINDER MAPPING OF SUBMESOSCALE VARIABILITY. CONDUCT RESEARCH, ALONG WITH MEMBERS OF THE OCEAN SURFACE TOPOGRAPHY SCIENCE TEAM (OSTST) AS WELL AS THE WIDER GEOPHYSICAL COMMUNITY, INTO THE PREDICTABILITY OF DEEP-OCEAN INTERNAL TIDES. PREPARE THE GROUNDWORK FOR HANDLING FUTURE SWOT MEASUREMENTS TO ALLOW SUCCESSFUL ESTIMATION OF TIDES. THE UNPRECEDENTED HIGH SPATIAL RESOLUTION OF SWOT DATA WILL, FOR EXAMPLE, REQUIRE REVISION OF STANDARD METHODS FOR TIDAL DATA ASSIMILATION. HELP WITH THE DESIGN OF ALGORITHMS FOR COMPUTING TIDAL CORRECTIONS TO SWOT DATA. FOR EXAMPLE, A COMPLEX FAMILY OF NESTED MODELS IS ENVISIONED IN ORDER TO PRODUCE THE MOST ACCURATE CORRECTIONS IN SHALLOW SEAS AND NEAR-COASTAL WATERS. Funding Only Action $61.0k 5/29/18